Abstract

Groundwater-quality assessment at contaminated sites often involves the use of short-screen (1.5 to 3 m) monitoring wells. However, even over these intervals considerable variation may occur in contaminant concentrations in groundwater adjacent to the well screen. This is especially true in heterogeneous dense non-aqueous phase liquid (DNAPL) source zones, where cm-scale contamination variability may call into question the effectiveness of monitoring wells to deliver representative data. The utility of monitoring wells in such settings is evaluated by reference to high-resolution multilevel sampler (MLS) wells located proximally to short-screen wells, together with sampling capture-zone modelling to explore controls upon well sample provenance and sensitivity to monitoring protocols. Field data are analysed from the highly instrumented SABRE research site that contained an old trichloroethene source zone within a shallow alluvial aquifer at a UK industrial facility. With increased purging, monitoring-well samples tend to a flow-weighted average concentration but may exhibit sensitivity to the implemented protocol and degree of purging. Formation heterogeneity adjacent to the well-screen particularly, alongside pump-intake position and water level, influence this sensitivity. Purging of low volumes is vulnerable to poor reproducibility arising from concentration variability predicted over the initial 1 to 2 screen volumes purged. Marked heterogeneity may also result in limited long-term sample concentration stabilization. Development of bespoke monitoring protocols, that consider screen volumes purged, alongside water-quality indicator parameter stabilization, is recommended to validate and reduce uncertainty when interpreting monitoring-well data within source zone areas. Generalised recommendations on monitoring well based protocols are also developed. A key monitoring well utility is their proportionately greater sample draw from permeable horizons constituting a significant contaminant flux pathway and hence representative fraction of source mass flux. Acquisition of complementary, high-resolution, site monitoring data, however, vitally underpins optimal interpretation of monitoring-well datasets and appropriate advancement of a site conceptual model and remedial implementation.

Highlights

  • Monitoring wells have been used extensively worldwide for the assessment of groundwater quality at contaminated sites (Barber and Davis, 1987; Basu et al, 2006; FDEP, 2008; Fretwell et al, 2006; Puls and Paul, 1997)

  • At dense nonaqueous phase liquid (DNAPL) contaminated sites, orders of magnitude changes in dissolved-phase concentrations may occur locally in sourcezone areas arising from the marked spatial variability in the occurrence of residual DNAPL contributing to dissolved-phase plume contaminaion

  • Objectives were: to evaluate proximal multilevel sampler (MLS) – monitoring well data within the existing SABRE research study field dataset obtained during baseline monitoring and bioremediation phases; to use numerical flow and transport modelling to inform the field-scale study interpretation and to explore sensitivities to monitoring well sample origins and sampling protocols; and, to consider the implications of sampling scale and well screen length for practitioners regarding the utility of monitoring wells, within DNAPL source zone areas

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Summary

Introduction

Monitoring wells have been used extensively worldwide for the assessment of groundwater quality at contaminated sites (Barber and Davis, 1987; Basu et al, 2006; FDEP, 2008; Fretwell et al, 2006; Puls and Paul, 1997). Whilst offering explanations for sample provenance (Hutchins and Acree, 2000; McDonald and Smith, 2009; Metcalf and Robbins, 2007; Puls and Paul, 1997; Reilly and LeBlanc, 1998; Sukop, 2000), typically lack the ideal of detailed corroborating data This notably includes data afforded by proximal high-resolution MLS transects that could be used to estimate groundwater flows and concentrations contributing to a well sample from the horizons screened. Objectives were: to evaluate proximal MLS – monitoring well data within the existing SABRE research study field dataset obtained during baseline monitoring and bioremediation phases; to use numerical flow and transport modelling to inform the field-scale study interpretation and to explore sensitivities to monitoring well sample origins and sampling protocols; and, to consider the implications of sampling scale and well screen length for practitioners regarding the utility of monitoring wells, within DNAPL source zone areas

Field site and historical field data overview
Numerical modelling approach
Observed MLS transect and monitoring well data
Provenance of monitoring well samples
Monitoring well sample bias towards preferential transport pathways
Numerical modelling results
Conclusions
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